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《Earth Science-journal of China University of Geosciences》 2003-01
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Demarcating Interval between Archean Group and Proterozoic Group and Ore-Forming Dynamical Transformation

DENG Jun 1,2 , SUN Zhong shi 3, WANG Jian ping 1, WANG Qing fei 1, WANG Xi chen 1, YAN Chang hai 1 (1.Department of Earth Science and Resource, China University of Geosciences, Beijing100083, China; 2.The Key Laboratory of Lithosphere Tectonics and Exploration (KLLTE), Ministry of Education, Beijing100083, China; 3.Department of Earth Science, Jilin University, Changchun130026, China)$$$$  
The narrowness and confusion of demarcating time between Archean and Proterozoic have kept deepening research on the early geology within great limits. Through determination demarcating and transiting criteria, the transformation of geo dynamics system between Archean and Proterozoic can be divided into four types: transformation from compressional to extensional system, from vertical to horizontal, of principal stress, from mantle plume to plate tectonics. The relatively outcomes which formed within 0.3~0.5 billions year of transformations includes eucaryote, radioelements, magma and ores. The partition between Archean and Proterozoic should have a transiting line, that can be limited in 2.20~2.80 Ga. The partition has close relation with major geological events, and this work brings a new edification to ore formation in depth.
【Fund】: 国家自然科学基金 (No .40 172 0 3 6) ;; 国家重点基础研究发展规划项目 (No.19990 43 2 0 6) ;; 教育部“科学技术研究重点项目 (No .0 10 3 7)” ;; “高等学校骨干教师资助计划”项目
【CateGory Index】: P611
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